Diffusion
Gas Diffusion
- Defined as the movement of gas from higher to lower partial pressure.
- Gradients for O2 and CO2 must be evaluated separately.
Dalton’s Law of Partial Pressures
- Each gas in a mixture has its own partial pressure.
- Ambient air: ~21% O2, ~78% N2.
- Barometric pressure at sea level: 760 mm Hg.
Calculation of Partial Pressure
- Formula: (P<em>B−47extmmHg)×F</em>gas=Pgas
- Example: For O2 in Boise (PB=690extmmHg):
- PIO2=(690−47)×0.21=135extmmHg
Alveolar Air Equation
- Modified equation: (P<em>B−47)×F</em>IO2−0.8PaCO2
- Clinical assumption: PaCO2≈PACO2.
Fick’s Law of Diffusion
- Factors: A (surface area), D (diffusion constant), T (thickness); influx formula: TA×D×(P<em>1−P</em>2).
- Higher thickness or lower surface area limits diffusion rate.
Capillary Transit Time
- Normal: 0.25 seconds required for O2 saturation, allowed time: 0.75 seconds.
- Oxygenation may decrease with conditions that thicken diffusion membranes.
Exercise and Disease Effects
- Exercise: increased cardiac output, potential limitation on oxygenation.
- Disease: thickening of membranes can cause oxygenation issues during exercise.
Diffusion Barriers for O2
- Components: Surfactant, alveolar epithelium, basement membrane, capillary endothelium, RBC membrane.
Influence of Conditions on Diffusion
- Emphysema: impairs diffusion.
- Elite athletes: risk of mild pulmonary edema affecting PaO2.
Interactions During Ventilation and Diffusion Changes
- Increased dead space (VD) decreases alveolar ventilation (VA), raises PaCO2, and lowers PAO2, affecting diffusion gradients.